Hiking and Walking Trails in and Around the Oxford Hills

Total Page:16

File Type:pdf, Size:1020Kb

Hiking and Walking Trails in and Around the Oxford Hills Hiking and Walking Trails in and around the Oxford Hills Hawk Mountain ½ mile, gentle climb with Ordway Grove is a walk through some of Streaked Mountain, is a short, rigorous upward views of the lakes region and white the oldest white pine and oak in the area. hike, with a few sections of shallow incline. Take Trailhead on the west side of Pleasant Street, mountitains. Off routes 35 & 37, take Mill Hill by Route 117 East from South Paris for 5.3 miles. Turn st two blocks north of Main. Norway Church, then 1 right on Fire Lane 95. Trailhead South onto Streaked Mountain Road. The trailhead is Is logging road on right at end of pavement. 0.5 miles past the power lines, which go straight up South Waterford the mountain. Buckfield Crocker Hill (known locally as Brown Mtn.) An easy 080.8 mile climb with nice views. Paris Hill Road to Mt. Mica Road. Follow 1.1 miles to gravel Thayer Road, 0.7 miles to trailhead. South Paris Roberts Farm Preserve Trails Roberts Farm Stevens Brook Trail A two‐mile trail between Preserve is located 2∕10th of a mile south of Lake Highland Lake and Long Lake in Bridgeton. Pennesseewassee off Roberts Road. Norway Follows Stevens Brook through downtown SingepoleMountain 1.3 miles, quarry and views over Halls Pond. 2 Miles east on Route 117 from Cornwall Nature Preserve on historic Paris Hill, Bridgton past scenic and historic natural areas. Ask for a trail map at library Information Desk. intersection with Route 119. South 0.5 miles on Brett this scenic preserve is ideal for nature study and Hill Road. At sharp corner go straight. South Paris photography. A trip to the preserve makes a Bridgton delightful family outing and picnic spot. About 2 Books about Hiking in Maine at Norway Library miles up Paris Hill Road from Route 26. Parking area AMC Maine Mtn. Guide 7th ed. M 917.41 AMC on the right. Paris Discover Acadia Nat’l Park M 917.41 Mon 50 Hikes in Southern Maine M 796.5 Gib Railroad Trail runs between Norway and South 50 Hikes in Southern and Coastal Maine M 796.5 Gib And a few outside the Oxford Hills Paris following a section of old railroad tracks. Hiker’s Guide to Maine M 796.5 Sey Portland Freedom Trail is a self‐guided walking Access from Danforth Street in Norway. At the Stop Hiking Maine M 796.5 Sey trail in downtown Portland currently comprised of sign bear right, on your immediate left you will see Katahdin: A Guide to Baxter St. Park M 917.41 Cla sixteen marked sites, recognizing people associated the Trail Sign. Approx 2/3 of a mile. Norway/Paris Maine Mountain Guide M 796.51 Mai with the Underground Railroad and anti‐slavery 100 Classic Hikes in New England: Maine, NH, VT, MA, movement in Portland. Information available at Mount Tire’m offers hikers a spectacular view of the RI and CT 796.5 Rom www.portlandfreedeomtrail.org . Portland Long Lake region and Presidential Range. Climbing Short Walks Along the Maine Coast M 917.41 Sad Sabattus Mountain a ¾ mile trail with great views time is about 40 minutes. At the junction of Rt. 35 WlkiWalking the MiMaine CtCoast M 796.5 Gib From Route 5 in Lovell, turn onto Sabattus Mountain and Rt. 37 in Waterford town center, turn on to Road. Go about 1.5 miles and bear right at the fork, Plummer Hill Road, next to Waterford Inn. Trailhead is onto a gravel road. Continue about 0.4 mile to the on left, unmarked. Waterford Sources: parking area on the right. Lovell Tips: Check weather reports to be prepared for http://www.amateur‐hikers.com changing conditions. Take water and a snack. Consider http://www. meliving. com/hiking/lakes.shtml Grafton Notch State Park has 3,100 acres on Route the least experienced hiker when determining your http://www.wfltmaine.org/ 26 between Newry and Upton. There are many scenic trail selection and pace. For more tips visit http://maineoutdoors.com/hiking/ areas and short walks in the area. Looking for a http://www.maine.gov/ifw/warden_service/safety.ht http://www.trails.com challenge? Old Speck mountain might be for you. It is Oxford Hills Magazine 2010‐2011, pg 47 ml#hiking Oxford Hills Trails Map, 2nd ed. Spring 2008 the third highest mountain, at 4180 feet, in the state. .
Recommended publications
  • Record Hill Responses to Comments
    Appendix B – Comment Response Record Hill Responses to Comments DOE received 35 individual comment submissions totaling 167 individual comments. DOE reviewed each comment received on the Record Hill EA and has grouped the comments into the following comment categories as noted in Table 1. The individual commenters are identified in Table 2. Table 1 – Comment Response Matrix Section Topic Commenter Numbers Comments 1. NEPA Process 3, 15, 16, 18, 24, 26, 30 3a, 15a, 15m, 16b, 18e, 24a, 24m, 26a, 26l, 30f Purpose and 1, 2, 12, 14, 18, 25, 27, 28, 1a, 2a, 2c, 12a, 14c, 18b, 18d, 18l, 25a, 25i, 27a, 28b, 28c, 2. Need 29, 33 28d, 28f, 29a, 29b, 29c, 33h, 33i Proposed 1a, 3b, 16d, 18c, 18f, 18g, 18h,18i, 18m, 18n, 18o, 18q, 18r, 3. Action and 1, 3, 16, 18, 25, 29, 33 25b, 25c, 25h, 29d, 33h Alternatives Water 5, 15, 18, 20, 23, 24, 25, 5a, 15c, 15e, 15g, 18t, 18u, 18v, 20f, 23a, 24c, 24e, 24f, 4. Resources 26, 30, 32 25e, 25g, 26c, 26e, 26f, 30d, 30e, 32a 5. Noise 11, 14, 17, 18, 19, 20, 35 11a, 11b, 14a, 14d, 17c, 18w, 19a, 20g, 35a Historic, Archaeological, 6. 20, 22 20b, 22b and Cultural Resources Aesthetic and Visual 12b, 15i, 18k, 18s, 18x, 18z, 18ab, 18ac, 20d, 20e, 24h, 7. 12, 15, 18, 20, 24, 26, 33 Resources and 26h, 33e Topography 8. Shadow Flicker 14 14b, 14d Occupational 9. Health and 11, 14, 15, 21, 24, 26 11a, 11b, 14d, 15h, 21a, 24g, 26g, Public Safety 3c, 5a, 5b, 13a, 13b, 15b, 15c, 15d, 16c, 17a, 17b, 17d, 17e, Biological 3, 5, 13, 15, 16, 17, 18, 24, 10.
    [Show full text]
  • Junior Newsletter, July 14, 2021
    JUNIOR TIMES July 14, 2021 Greetings from Junior Winona! We have had another terrific week that can only be summarized by the fact that, regardless of the weather, Junior campers always know how to have the best time and our counselors know how to create engaging activities. While we had a bit of rain, we also saw a fair amount of sunshine that allowed us to be outside and celebrate our new squads, welcome CITs and send many trips out and about. On Wednesday morning, Uncle Lime, Aunt Wren and Uncle Ben took the BAT Barge across Moose Pond to hike part of Pleasant Mountain and find the Needles Eye. Campers Mattias Calderon Chubb, Eliot Harris, Brody Watkins, Connor Kirkham, Blake Alexander-Pletzke, Lucas Lapin, Will Lothian, Victor Rannik and Mark Weaver took part on this local hike exploring some stunning geological features of the mountain. Thursday morning, a canoe trip left the beach for a day trip up to Newt’s Isle (an island located in the northern basin of Moose Pond). Campers, Mark Weaver, Leo Milberg, Finn Stevenson, James Golden, David Gengler, Jackson Tankersly, Francis Rangel and Lochlann O’Connell, were led by counselors Uncle Josef, Uncle Lee and CIT Lucas. The counselors and campers had great weather and were able to enjoy the afternoon on the calm waters of Moose Pond. Friday evening was Movie Night in Junior! The campers enjoyed eating popcorn and watching Ice Age: Dawn of the Dinosaurs. The cloudy weather made for a perfect movie night here at camp. Campfire is always a wonderful community event on Saturday evenings.
    [Show full text]
  • Old Speck Mountain Appalachian Trail and Eyebrow Loop – 6.2 Miles Round Trip, Advanced
    Old Speck Mountain Appalachian Trail and Eyebrow Loop – 6.2 miles round trip, Advanced ld Speck Mountain, the northeastern terminus of the Mahoosuc Range, has long been a popular O hike along the Appalachian Trail. Here, evidence from the last glaciation is everywhere, and in- cludes scoured bedrock, Speck Pond tarn, erratic boulders and even the massive carved valley of Grafton Notch. While its glacial history is part of what gives the rugged landscape of Western Maine its charac- ter, exposed bedrock and shallow soils, harsh high elevation climate conditions, and catastrophic disturb- ance events have also shaped the variety of vegetation and habitats found here. The forests that have de- veloped are adapted to these unique soil and climate conditions. Temperate northern hardwood forest is prevalent at the base of Old Speck. Deep, fine grained soils devel- oped from the sediment eroded from slopes above, support hardwood species including American beech, yellow birch and sugar maple. Ascending in elevation, harsh climate conditions lead to a change in forest type. Red spruce and balsam fir are increasingly common, and hardwood species diminish. Nearing Old Speck’s peak, even red spruce becomes scarce. Here, heart-leaved-paper birch, balsam fir and scattered black spruce, highly tolerant of harsh weather and frequent disturbance, are the dominant canopy spe- cies. ————————————————————— Trailhead -70.94726, 44.59018 The parking lot offers an excellent view of the cliffs on the east side of Old Speck. From the trailhead, there is a great view of the Eyebrow Cliffs and during the summer one may observe peregrine falcons, a species once extirpated from Maine due to the use of the pesticide DDT.
    [Show full text]
  • Geologic Site of the Month: Glacial and Postglacial
    Geology of Grafton Notch State Park Maine Geological Survey Maine Geologic Facts and Localities November, 2001 Glacial and Postglacial Geology of Grafton Notch State Park 44o 35‘ 36.21“ N, 70o 56‘ 52.27“ W Text by Woodrow B. Thompson Maine Geological Survey, Department of Agriculture, Conservation & Forestry 1 Geology of Grafton Notch State Park Maine Geological Survey Introduction Grafton Notch State Park (Figure 1) has a spectacular combination of scenery and geology, with landforms illustrating the power of glacial ice and running water in shaping Maine's landscape. Deeply eroded glacial valleys, high cliffs, narrow stream gorges, and potholes are among the striking features that can be seen within the park. These sites are easily accessible along Route 26, with parking and trails conveniently located for group field trips. Maine Geological Survey Map USGS Map by Figure 1. Map of Grafton Notch State Park. Maine Geological Survey, Department of Agriculture, Conservation & Forestry 2 Geology of Grafton Notch State Park Maine Geological Survey Logistics The geology of the park also raises some challenging questions concerning the age and origin of Screw Auger Falls and the other waterfalls and gorges seen on this trip. These features are not well understood (even by geologists working in Maine!), so they lend themselves to thought-provoking discussions among teachers and students. Permission: The park is maintained by the Bureau of Parks and Lands, Maine Department of Agriculture, Conservation and Forestry. No permission is required to visit. Further information is available from the park headquarters (207-824-2912, May 15 - October 15) or the regional office (207-624-6080, year- round).
    [Show full text]
  • Carboniferous Metamorphism on the North (Upper) Side of the Sebago Batholith
    University of New Hampshire University of New Hampshire Scholars' Repository New England Intercollegiate Geological NEIGC Trips Excursion Collection 1-1-1986 Carboniferous metamorphism on the north (upper) side of the Sebago Batholith Guidotti, C.V. Gibson, D. Lux, D.R. DeYoreo, J. Cheney, J.T. Follow this and additional works at: https://scholars.unh.edu/neigc_trips Recommended Citation Guidotti, C.V.; Gibson, D.; Lux, D.R.; DeYoreo, J.; and Cheney, J.T., "Carboniferous metamorphism on the north (upper) side of the Sebago Batholith" (1986). NEIGC Trips. 404. https://scholars.unh.edu/neigc_trips/404 This Text is brought to you for free and open access by the New England Intercollegiate Geological Excursion Collection at University of New Hampshire Scholars' Repository. It has been accepted for inclusion in NEIGC Trips by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. TRIP C-4 m It£ NORTH ( UPPER ) SIDE Q£ IME. SEBAGO By C.V. Guldottl1, D. Gibson1, D.R. Lux1,0J. De Yoreo1, 2 and J.T. Cheney ( U n l v . of Maine, Orono, Maine. (2) Amherst College, Amherst, MA Until recently the high-grade metamorphism In western Maine was routinely accepted as Devonian In age. Initially, only a single Devonian event was assumed and Pankiwskyj (1965) appears to have been the first worker to tentatively suggest the existence of more than one Devonian metamorphism. Subsequently, Guldottl (1970) described explicitly at least three Devonian metamorphisms. The most recent overviews of the Devonian metamorphic events In central and western Maine have been given by Holdaway et al.
    [Show full text]
  • Styles of Metamorphism with Depth in the Central Acadian High, New
    STYLES OF ACADIAN METAMORPHISM WITH DEPTH IN THE CENTRAL ACADIAN HIGH, NEW ENGLAND A Field Trip Honoring J. B. Thompson, Jr. by C. Page Chamberlain!, Henry N. Berry 1v2, John T. Cheney3, M. P. Dickenson4, John M. Ferry5, Charles V. Guidotti6, Kurt Hollocher7,Philip H. Osberg6, Peter Robinson2, Douglas Rumble, III8, Jennifer A. Thomson2 and Robert J. Tracy9 C. Page Chamberlain 1 and Peter Robinson2 Editors I Department of Earth Sciences, Dartmouth College, Hanover, NH 03755 2 Department of Geology and Geography, University of Massachusetts, Amherst, MA 01003 3 Department of Geology, Amherst College, Amherst, MA 01002 4 EC Jordan, 261 Commercial St., P. 0. Box 7050, Portland, ME 04112 5 Department of Earth and Planetary Sciences, The Johns Hopkins University, Baltimore MD 21218 6 Department of Geological Sciences, University of Maine, Orono, ME 04469 7 Department of Geology, Union College, Schenectady, NY 12308 8 Geophysical Laboratory, Carnegie Institution, 2801 Upton St., NW, Washington, D. C. 20008 9 Department of Geological Sciences, Virginia Polytechnic Institute and State University, Blacksburg, VA 24061 September 8-11, 1989 Contribution No. 63, Department of Geology and Geography University of Massachusetts, Amherst, Massachusetts iii INTRODUCTION For over three decades, Jim Thompson has led students on field trips across the northern Appalachians of New England. Typically, this trip was run across the tectonic grain, extending from the Grenville basement of the Adirondacks to the high-grade Devonian gneisses of New Hampshire. Because JBT's field trips were across strike traverses the emphasis was both on the metamorphism and tectonics of the Appalachians. During the organization of the field trip that we are now on we discussed whether or not to run the same field trip in honor of JBT.
    [Show full text]
  • R9 Community Conservation Assessment
    Community Conservation Assessment for White Mountain Alpine Community USDA Forest Service, Eastern Region April 2003 Catherine Rees 719 Main St. Laconia, NH 03247 603-528-8721 WHITE MOUNTAIN NATIONAL FOREST Community Conservation Assessment for White Mountain Alpine Community 1 This document was prepared to compile the published and unpublished information on the subject community to serve as a Conservation Assessment for the Eastern Region of the Forest Service. It does not represent a management decision by the U.S. Forest Service. Though the best scientific information available was used and subject experts were consulted in preparation of this document, it is expected that new information will arise. In the spirit of continuous learning and adaptive management, if you have information that will assist in conserving the subject community, please contact the Eastern Region of the Forest Service Threatened and Endangered Species Program at 310 Wisconsin Avenue, Suite 580 Milwaukee. Wisconsin 53203. Community Conservation Assessment for White Mountain Alpine Community 2 Table of Contents EXECUTIVE SUMMARY..................................................................................... 4 COMMUNITY CLASSIFICATION SYSTEM AND SYNONYMS ................. 5 DESCRIPTION OF COMMUNITY..................................................................... 7 COMMUNITY ECOLOGY/ENVIRONMENTAL CONDITIONS ................ 16 RANGE OF NATURAL VARIABILITY: COMMUNITY DISTRIBUTION AND CONDITIONS ............................................................................................
    [Show full text]
  • Bibliography of Maine Geology 1672 - 1972 Maine Department of Conservation
    Maine State Library Digital Maine Geology Documents Geological Survey 1982 Bibliography of Maine Geology 1672 - 1972 Maine Department of Conservation Maine Geological Survey Arthur M. Hussey II Bowdoin College Follow this and additional works at: https://digitalmaine.com/geo_docs Recommended Citation Maine Department of Conservation; Maine Geological Survey; and Hussey, Arthur M. II, "Bibliography of Maine Geology 1672 - 1972" (1982). Geology Documents. 3. https://digitalmaine.com/geo_docs/3 This Text is brought to you for free and open access by the Geological Survey at Digital Maine. It has been accepted for inclusion in Geology Documents by an authorized administrator of Digital Maine. For more information, please contact [email protected]. M , D 0c.G34.8:r ^ / E67fl7A2TE U B R A R Y Hussey, Arthur M. Biblio raphy of Maine oeolo 1672-1972 Maine Geological Survey DEPARTMENT OF CONSERVATION Augusta, Maine 04333 BIBLIOGRAPHY OF MAINE GEOLOGY 1672 - 1972 Compiled and Edited by Arthur M. Hussey II Bowdoin College 19 8 2 OCT 5 1989 Maine Geological Survey DEPARTMENT OF CONSERVATION Augusta, Maine 04333 BIBLIOGRAPHY OF MAINE GEOLOGY 1672 - 1972 Compiled and Edited by Arthur M. Hussey II Bowdoin College Reprinted 1982 ( First printing 1974 ) Walter A. Anderson, State Geologist Preface This bibliography and index to Maine geology supercedes all bibliographies and supplements previously published by the Maine Geological Survey, the last supplement of which included articles through 1966. All major journals and government publications dating from January 1967 through December 1972 were searched for references relating to the geology of Maine (including the Gulf of Maine area). In addition, much use was made of the Bibliography and Index of North American Geology for the years 1967 through 1969 published by the U.
    [Show full text]
  • Stratigraphy, Geochronology, and Accretionary Terrane Settings of Two Bronson Hill Arc Sequences, Northern New England
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by DigitalCommons@University of Nebraska University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln USGS Staff -- Published Research US Geological Survey 2003 Stratigraphy, geochronology, and accretionary terrane settings of two Bronson Hill arc sequences, northern New England Robert H. Moench U.S. Geological Survey, [email protected] John N. Aleinikoff U.S. Geological Survey Follow this and additional works at: https://digitalcommons.unl.edu/usgsstaffpub Part of the Earth Sciences Commons Moench, Robert H. and Aleinikoff, John N., "Stratigraphy, geochronology, and accretionary terrane settings of two Bronson Hill arc sequences, northern New England" (2003). USGS Staff -- Published Research. 436. https://digitalcommons.unl.edu/usgsstaffpub/436 This Article is brought to you for free and open access by the US Geological Survey at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in USGS Staff -- Published Research by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Physics and Chemistry of the Earth 28 (2003) 113–160 www.elsevier.com/locate/pce Stratigraphy, geochronology, and accretionary terrane settings of two Bronson Hill arc sequences, northern New England q,qq Robert H. Moench a,*, John N. Aleinikoff b a US Geological Survey, MS 905, Federal Center, Denver, CO 80225, USA b US Geological Survey, MS 963, Federal Center, Denver, CO 80225, USA Abstract The Ammonoosuc Volcanics, Partridge Formation, and the Oliverian and Highlandcroft Plutonic Suites of the Bronson Hill anticlinorium (BHA) in axial New England are widely accepted as a single Middle to Late Ordovician magmatic arc that was active during closure of Iapetus.
    [Show full text]
  • Appalachian Trail Vital Signs
    National Park Service U.S. Department of the Interior Northeast Region Boston, Massachusetts Appalachian Trail Vital Signs Technical Report NPS/NER/NRTR--2005/026 ON THE COVER Androscoggin River, ME Blood Mountain Sunset, GA Laurel Falls, TN Mt Katahdin, ME © Photos by Joe Cook Appalachian Trail Vital Signs Technical Report NPS/NER/NRTR--2005/026 Greg Shriver1, Tonnie Maniero2, Kent Schwarzkopf3, Dan Lambert4, Fred Dieffenbach1, Don Owen3, Y. Q. Wang5, Joy Nugranad- Marzilli5, Geri Tierney6, Casey Reese3, Theresa T. Moore1 1National Park Service Inventory and Monitoring Program 54 Elm Street Woodstock, Vermont 05091 2National Park Service Northeast Region 15 State Street Boston, Massachusetts 02109 3National Park Service Appalachian National Scenic Trail Harpers Ferry Center Harpers Ferry, West Virginia 25425 4Vermont Institute of Natural Science Conservation Biology Department 2723 Church Hill Road Woodstock, Vermont 05091 5University of Rhode Island Department of Natural Resource Science Kingston, Rhode Island 02881 6State University of New York College of Environmental Science and Forestry 1 Forestry Drive Syracuse, New York 13210 November 2005 U.S. Department of the Interior National Park Service Northeast Region Boston, Massachusetts The Northeast Region of the National Park Service (NPS) comprises national parks and related areas in 13 New England and Mid- Atlantic states. The diversity of parks and their resources are reflected in their designations as national parks, seashores, historic sites, recreation areas, military parks, memorials, and rivers and trails. Biological, physical, and social science research results, natural resource inventory and monitoring data, scientific literature reviews, bibliographies, and proceedings of technical workshops and conferences related to these park units are disseminated through the NPS/NER Technical Report (NRTR) and Natural Resources Report (NRR) series.
    [Show full text]
  • Geologic Map of the Kenneabago Lake Quadrangle, Franklin County, Maine
    DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP 1-2058 U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE KENNEABAGO LAKE QUADRANGLE, FRANKLIN COUNTY, MAINE By Eugene L. Boudette INTRODUCTION phased rocks as Early to Middle Proterozoic remains valid and the Jim Pond is older than the Ammonoosuc (see also Baudette, 1982, Previous work and Baudette and Boone, 1976). The earliest reconnaissance geologic investigations in this part of Silurian rocks older than those of the Moose River synclinorium Maine were by Jackson (1837, 1839), Holmes and Hitchcock occur in the quadrangle. A northwest-trending marine onlap during (1861, 1862), Hitchcock and Huntington (1874), and Hitchcock the Silurian was established (U.S. Geological Survey, 1965). (1877, 1878). Other early studies included the granitic plutons by Harwood and Berry (1967) determined a Middle Ordovician age Dale (1907), the Rangeley Conglomerate by Smith (1923), and for rocks in the Cupsuptic quadrangle (fig. 1) on regional strike with the bedrock geology by Keith (1933). a unit in the southwestern corner of the Kennebago Lake quad­ Studies related to mineral occurrences in the region were rangle. Moench (1969) defined and mapped the Upper Ordovi­ reported by Pratt and Allen (1949) on agricultural limestone, and cian(?) and Quimby and Greenvale Cove Formations in the by Wing and Dawson (1949) and Wing (1951a,b) on asbestos, Rangeley quadrangle. The Rangeley Formation and Perry Moun­ serpentinite, and greenstone. Many independent mining compa­ tain Formations were revised and defined by Osberg and others nies actively studied base-metal deposits during the period from (1968) in their description of the Kearsarge-central Maine syncli­ 1950 to 1968.
    [Show full text]
  • The Impact of Existing and Potential Wind Power Development on High-Value Scenic Resources in Maine
    The impact of existing and potential wind power development on high-value scenic resources in Maine APPALACHIAN MOUNTAIN CLUB The impact of existing and potential wind power development on high-value scenic resources in Maine David Publicover and Catherine Poppenwimer Appalachian Mountain Club Research Department Gorham, NH AMC Technical Report 19-1 November 2019 Acknowledgements Funding for this project was provided by the Horizon Foundation, the Sally Mead Hands Foundation and five individual donors. We thank them for the support. We also thank our Maine Audubon Society colleagues Sarah Haggerty, Eliza Donohue, Sally Stockwell and Susan Gallo for their assistance and support during this project. Suggested citation Publicover, D. and C. Poppenwimer. 2019. The impact of existing and potential wind power development on high-value scenic resources in Maine. AMC Technical Report 19-1. Appalachian Mountain Club, Gorham, NH. This study was undertaken as part of a collaborative project with Maine Audubon Society. MAS has released a companion report titled “Renewable Energy and Wildlife in Maine: Avoiding, Minimizing and Mitigating Impacts to Wildlife and Habitat from Solar, Wind and Transmission Facilities”, available at https://www.maineaudubon.org/advocacy/climate-energy/. EXECUTIVE SUMMARY Overview This project was undertaken to better understand the visual impact of existing wind power projects on high-value scenic resources in Maine (especially mountains and large lakes), how these impacts have been evaluated in permitting decisions, and the potential for future impacts to these resources from proposed or potential projects. The information was developed to better inform the on-going discussion on the future development of this renewable energy technology in Maine’s landscape.
    [Show full text]